Three-dimensionality in transitioning mixing layers, in the form of st
reamwise vortical structures, is now well established and understood.
In the present investigation, the effects of velocity ratio, or more p
recisely of velocity difference across the layer, on the near-field ge
neration and development of three-dimensionality in two-stream mixing
layers have been investigated for the first rime. Detailed time-averag
ed velocity measurements were obtained using a single rotatable cross-
wire probe on fine cross-plane grids at four streamwise locations in t
he near-field region. The effects of five velocity ratios, ranging fro
m r = 0.5 to 0.9, were investigated by keeping the velocity of one str
eam constant while varying that of the other. The results indicate tha
t the mixing layer three-dimensionality is strongest for the mixing la
yer with the lowest velocity ratio. The peak mean streamwise vorticity
levels decrease with increasing velocity ratio at all the streamwise
locations investigated. However, the rate of decrease is highest at th
e most upstream station and it decreases with increasing downstream di
stance. The mean streamwise vorticity contours at the first station sh
aw that their distribution is quite similar at the different velocity
ratios, implying that the generating mechanism and initial disturbance
fields remain unchanged with velocity ratio. However, it is conceivab
le that the amount of stretching in the braid regions due to the spanw
ise vortical structures is affected by velocity ratio. As the velocity
ratio decreases land the velocity difference across the layer increas
es), stronger spanwise rollers are generated which increase the amount
of stretching in the braid regions and hence the streamwise vorticity
is amplified. The splitter plate wake has a lasting effect on the thr
ee-dimensional structure of the mixing layers at the higher velocity r
atios, The presence and effects of the wake are clearly seen in the me
an velocity, mean streamwise vorticity and Reynolds stress contours. (
C) 1998 Elsevier Science Inc. All rights reserved.